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Formation Water Genesis Mechanism of Deep Tight Sandstone Gas Reservoirs in the Southern Ordos Basin and Its Indication for Development.

作者信息

Zhang Jianting, Wang Ruifei, Jia Ailin, Feng Naichao, Liu Ruohan, Wang Mengqi

机构信息

School of Petroleum Engineering, Xi'an Shiyou University, Xi'an, Shaanxi 710016, China.

Engineering Research Center of Development and Management for Low to Ultra-Low Permeability Oil & Gas Reservoirs in West China, Ministry of Education, Xi'an, 710016, China.

出版信息

ACS Omega. 2025 Jan 6;10(1):1809-1828. doi: 10.1021/acsomega.4c10171. eCollection 2025 Jan 14.

DOI:10.1021/acsomega.4c10171
PMID:39829599
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC11740109/
Abstract

By analyzing the chemical characteristics of the formation water in the tight sandstone reservoirs of the P2x8 and P1s1 in the southern Ordos Basin, combined with rock mineral composition, reservoir physical properties, and well gas testing data, the genesis mechanism of formation water and its guiding role in gas reservoir development were discussed. The results show that the formation water is derived from the mixture of syngenetic seawater and meteoric water and has undergone remarkable modification by water-rock interactions, showing characteristics of Ca enrichment and Mg and SO depletion. The albitization of plagioclase in reservoir rock components causes Ca excess and Na deficiency in formation water, while the chloritization of albite leads to the increase of Na. The dolomitization of calcite contributes to the decrease of Mg in the formation water, while later ankerite formation makes the correlation of Ca excess-Mg deficit worse. In addition, the chloritization of dolomite and the formation of calcified debris by the metasomatism of ferrocalcite further increase the Ca content of the formation water. Fe reduction and pyrite formation in reservoir minerals reduce the concentration of SO . The study also show that reservoirs endowed with Ca-Cl type formation water has more production potential. Chlorite fill, argillaceous debris, and calcareous debris are negatively correlated with face rate, porosity, and permeability. It is innovatively proposed that the specific formation chemical characteristics combinations and can effectively characterize reservoir porosity and permeability, while combinations and are strongly correlated with gas production and water production. In conclusion, the hydrochemical characteristics of geological formations are important references for reservoir evaluation and development indicators, which is helpful to accurately evaluate the development potential of reservoirs and guide exploration strategies of gas reservoirs.

摘要
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8685/11740109/4eb36b623184/ao4c10171_0014.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8685/11740109/59c5a6cb1750/ao4c10171_0001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8685/11740109/3e306b1886c3/ao4c10171_0002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8685/11740109/0f051dd98359/ao4c10171_0003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8685/11740109/76d5aef27a55/ao4c10171_0004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8685/11740109/52ca7e7c8595/ao4c10171_0005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8685/11740109/3dca7c56ae9a/ao4c10171_0006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8685/11740109/fc68b19a35e6/ao4c10171_0007.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8685/11740109/87819ee69ff0/ao4c10171_0008.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8685/11740109/24fab6cc24ae/ao4c10171_0009.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8685/11740109/a982ab360a60/ao4c10171_0010.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8685/11740109/0365ef2a5fc1/ao4c10171_0011.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8685/11740109/a253f1693e3a/ao4c10171_0012.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8685/11740109/363fe763be8e/ao4c10171_0013.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8685/11740109/4eb36b623184/ao4c10171_0014.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8685/11740109/59c5a6cb1750/ao4c10171_0001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8685/11740109/3e306b1886c3/ao4c10171_0002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8685/11740109/0f051dd98359/ao4c10171_0003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8685/11740109/76d5aef27a55/ao4c10171_0004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8685/11740109/52ca7e7c8595/ao4c10171_0005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8685/11740109/3dca7c56ae9a/ao4c10171_0006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8685/11740109/fc68b19a35e6/ao4c10171_0007.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8685/11740109/87819ee69ff0/ao4c10171_0008.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8685/11740109/24fab6cc24ae/ao4c10171_0009.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8685/11740109/a982ab360a60/ao4c10171_0010.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8685/11740109/0365ef2a5fc1/ao4c10171_0011.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8685/11740109/a253f1693e3a/ao4c10171_0012.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8685/11740109/363fe763be8e/ao4c10171_0013.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8685/11740109/4eb36b623184/ao4c10171_0014.jpg

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本文引用的文献

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Indication of Formation Water Geochemistry for Hydrocarbon Preservation: New Applications of Machine Learning in Tight Sandstone Gas Reservoirs.地层水地球化学对油气保存的指示作用:机器学习在致密砂岩气藏中的新应用
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锶同位素作为水-岩石相互作用、混合过程的示踪剂以及法国科西嘉博尼法乔(Bonifacio)花岗岩-碳酸盐滨海含水层地下水滞留时间的指示剂。
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